Mid-Ocean Ridge: The longest chain of mountains in the world. Sonar: A device that bounces sound waves off underwater objects and then record the echoes of these waves. Sea-floor spreading: The process that continually adds new material to the ocean floor. Deep-ocean trenches: Deep underwater canyons. Subduction:The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle.
Outline
Introduction
The Ocean Floor
Freezing temperatures
Crushing pressure
Most bizarre creatures ever found.
Ex. Giant red tube worms, Giant clams nearly a meter across and strange spider-like crabs
Mapping the Mid-Ocean Ridge
Mid-Ocean Ridge is the longest chain of mountains in the world.
Goes through all the oceans and around the world ( Only underwater )
Use sonar to locate it.
Sonar is a device that bounces sound waves off underwater objects and then records the echoes of these waves.
Evidence for Sea-floor Spreading
At the mid-ocean ridge, molten material rises from the mantle and erupts spreading molten material and pushing older rock to both sides of the ridge.
Harry Hess, an American geologist, was one of the scientists who studied the mid-ocean ridge.
Hess called the process that continually adds new material to the ocean floor is called sea-floor spreading.
Evidence from Molten Material
In the 1960's, scientists found evidence of new material.
Scientists found pillow like lava ( forms when magma cools very quickly) on the ocean floor.
Went down in a submersible named Alvin.
Evidence from Magnetic Stripes
Scientists have found patterns in the rocks on the ocean floor.
Evidence shows that the Earth's poles have reversed themselves.
This last happened 780,000 years ago.
ocean floor lies in a pattern of magnetic stripes.
These stripes hold the record of reversals in the Earth's magnetic field.
Evidence from Drilling Samples
The Glomar Challenger, a drilling ship built in 1968, sent drilling pipes through the water to dig deep holes in the ocean floor.
It sent the pipes 6 kilometers down.
Samples were brought up through the pipes.
Subduction at Deep-Ocean Trenches
A deep ocean trench forms where the oceanic crust bends downward.
Suduction occurs at these places.
At deep ocean trenches, subduction allows part of the ocean floor to sink back into the mantle.
Subduction and Earth's Oceans
The ocean floor is renewed every 200 million years.
This is the time it takes the rocks to form at the mid ocean ridge.
Subduction in the Pacific Ocean
The Pacific Ocean covers one-third of our planet and it is shrinking.
The Pacific Ocean has a lot of trenches.
A deep ocean trench swallows more oceanic than the mid-ocean ridge can produce.
Then if the mid-ocean ridge does not add new crust fast enough it will shrink.
This is what is happening to the Pacific Ocean.
Subduction in the Atlantic Ocean
The Atlantic Ocean is expanding.
Unlike the Pacific, the Atlantic only has a few short trenches.
As a result the new ocean floor has nowhere to go.
Table of Contents
1.4 Sea-Floor Spreading
Vocabulary
Mid-Ocean Ridge: The longest chain of mountains in the world.
Sonar: A device that bounces sound waves off underwater objects and then record the echoes of these waves.
Sea-floor spreading: The process that continually adds new material to the ocean floor.
Deep-ocean trenches: Deep underwater canyons.
Subduction:The process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle.
Outline
Introduction
Mapping the Mid-Ocean Ridge
Evidence for Sea-floor Spreading
Evidence from Molten Material
- In the 1960's, scientists found evidence of new material.
- Scientists found pillow like lava ( forms when magma cools very quickly) on the ocean floor.
Went down in a submersible named Alvin.Evidence from Magnetic Stripes
Evidence from Drilling Samples
Subduction at Deep-Ocean Trenches
Subduction and Earth's Oceans
Subduction in the Pacific Ocean
Subduction in the Atlantic Ocean